Amino acids dominate diffusive nitrogen fluxes across soil depths in acidic tussock tundra
Peter M. Homyak, Eric Slessarev, Shannon B. Hagerty, Aral C. Greene, Kenneth Marchus, Kelsey Dowdy, Sadie L. Iverson, Joshua P. Schimel
Abstract
Summary Organic nitrogen (N) is abundant in soils, but early conceptual frameworks considered it nonessential for plant growth. It is now well recognised that plants have the potential to take up organic N. However, it is still unclear whether plants supplement their N requirements by taking up organic N in situ : at what rate is organic N diffusing towards roots and are plants taking it up? We combined microdialysis with live‐root uptake experiments to measure amino acid speciation and diffusion rates towards roots of Eriophorum vaginatum . Amino acid diffusion rates (321 ng N cm −2 h −1 ) were c . 3× higher than those for inorganic N. Positively charged amino acids made up 68% of the N diffusing through soils compared with neutral and negatively charged amino acids. Live‐root uptake experiments confirmed that amino acids are taken up by plants (up to 1 µg N g −1 min −1 potential net uptake). Amino acids must be considered when forecasting plant‐available N, especially when they dominate the N supply, and when acidity favours proteolysis over net N mineralisation. Determining amino acid production pathways and supply rates will become increasingly important in projecting the extent and consequences of shrub expansion, especially considering the higher C : N ratio of plants relative to soil.